Touching the detachment (Ockov Fault, Barrandian, Czech Republic)
N.º 29, International Meeting of Young Researchers in Structural Geology and Tectonics (Part 1)
N.º 29

Touching the detachment (Ockov Fault, Barrandian, Czech Republic)

International Meeting of Young Researchers in Structural Geology and Tectonics (Part 1)
  • J. Černý
  • R. Melichar
  • M. Knižek
  • J. Janečka
J. Černý
R. Melichar
M. Knižek
J. Janečka
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Como Citar

Černý, J., Melichar, R., Knižek, M., & Janečka, J. (2011). Touching the detachment (Ockov Fault, Barrandian, Czech Republic). TRABAJOS DE GEOLOGÍA, 29(29). Obtido de https://reunido.uniovi.es/index.php/TDG/article/view/296
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Resumo

The Prague Synform (Ordovician to Devonian) was folded and thrusted during the Variscan orogeny. This paper is focused on one of these thrusts: the Ockov Fault. The creation of a stratigraphic separation diagram and detailed study of new tunnel exposures has brought about the recognition of the eastern prolongation of the fault, as well as its flat-ramp-flat geometry and thrusting nature.
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